Average Weather in April in Palo Seco (El Gato) Mexico
Daily high temperatures are around 88°F, rarely falling below 77°F or exceeding 99°F.
Daily low temperatures increase by 4°F, from 58°F to 61°F, rarely falling below 50°F or exceeding 67°F.
For reference, on May 10, the hottest day of the year, temperatures in Palo Seco (El Gato) typically range from 63°F to 90°F, while on January 7, the coldest day of the year, they range from 47°F to 75°F.
Average High and Low Temperature in April
The figure below shows you a compact characterization of the hourly average temperatures for the quarter of the year centered on April. The horizontal axis is the day, the vertical axis is the hour of the day, and the color is the average temperature for that hour and day.
Average Hourly Temperature in April
The month of April in Palo Seco (El Gato) experiences essentially constant cloud cover, with the percentage of time that the sky is overcast or mostly cloudy remaining about 39% throughout the month. The highest chance of overcast or mostly cloudy conditions is 41% on April 9.
The clearest day of the month is April 26, with clear, mostly clear, or partly cloudy conditions 63% of the time.
For reference, on September 15, the cloudiest day of the year, the chance of overcast or mostly cloudy conditions is 72%, while on May 23, the clearest day of the year, the chance of clear, mostly clear, or partly cloudy skies is 68%.
Cloud Cover Categories in April
A wet day is one with at least 0.04 inches of liquid or liquid-equivalent precipitation. In Palo Seco (El Gato), the chance of a wet day over the course of April is very rapidly increasing, starting the month at 7% and ending it at 16%.
For reference, the year's highest daily chance of a wet day is 42% on September 4, and its lowest chance is 4% on December 13.
Probability of Precipitation in April
To show variation within the month and not just the monthly total, we show the rainfall accumulated over a sliding 31-day period centered around each day.
The average sliding 31-day rainfall during April in Palo Seco (El Gato) is increasing, starting the month at 0.7 inches, when it rarely exceeds 2.4 inches, and ending the month at 1.5 inches, when it rarely exceeds 3.5 inches or falls below 0.1 inches.
Average Monthly Rainfall in April
Over the course of April in Palo Seco (El Gato), the length of the day is increasing. From the start to the end of the month, the length of the day increases by 35 minutes, implying an average daily increase of 1 minute, 13 seconds, and weekly increase of 8 minutes, 28 seconds.
The shortest day of the month is April 1, with 12 hours, 23 minutes of daylight and the longest day is April 30, with 12 hours, 58 minutes of daylight.
Hours of Daylight and Twilight in April
The latest sunrise of the month in Palo Seco (El Gato) is 7:33 AM on April 1 and the earliest sunrise is 24 minutes earlier at 7:09 AM on April 30.
The earliest sunset is 7:56 PM on April 1 and the latest sunset is 11 minutes later at 8:07 PM on April 30.
Daylight saving time (DST) starts at 3:00 AM on April 1, 2018, shifting sunrise and sunset to be an hour later.
For reference, on June 21, the longest day of the year, the Sun rises at 6:57 AM and sets 13 hours, 30 minutes later, at 8:27 PM, while on December 21, the shortest day of the year, it rises at 7:15 AM and sets 10 hours, 46 minutes later, at 6:01 PM.
Sunrise & Sunset with Twilight and Daylight Saving Time in April
We base the humidity comfort level on the dew point, as it determines whether perspiration will evaporate from the skin, thereby cooling the body. Lower dew points feel drier and higher dew points feel more humid. Unlike temperature, which typically varies significantly between night and day, dew point tends to change more slowly, so while the temperature may drop at night, a muggy day is typically followed by a muggy night.
The chance that a given day will be muggy in Palo Seco (El Gato) is increasing during April, rising from 2% to 10% over the course of the month.
For reference, on June 20, the muggiest day of the year, there are muggy conditions 17% of the time, while on January 9, the least muggy day of the year, there are muggy conditions 0% of the time.
Humidity Comfort Levels in April
This section discusses the wide-area hourly average wind vector (speed and direction) at 10 meters above the ground. The wind experienced at any given location is highly dependent on local topography and other factors, and instantaneous wind speed and direction vary more widely than hourly averages.
The average hourly wind speed in Palo Seco (El Gato) is essentially constant during April, remaining within 0.1 miles per hour of 8.2 miles per hour throughout.
For reference, on June 27, the windiest day of the year, the daily average wind speed is 8.4 miles per hour, while on December 2, the calmest day of the year, the daily average wind speed is 6.3 miles per hour.
The highest daily average wind speed during April is 8.3 miles per hour on April 1.
Average Wind Speed in April
Wind Direction in April
Definitions of the growing season vary throughout the world, but for the purposes of this report, we define it as the longest continuous period of non-freezing temperatures (≥ 32°F) in the year (the calendar year in the Northern Hemisphere, or from July 1 until June 30 in the Southern Hemisphere).
While it does not do so every year, freezing temperatures are seen in Palo Seco (El Gato) over some winters. The day least likely to be in the growing season is January 4, with a 73% chance.
Time Spent in Various Temperature Bands and the Growing Season in April
Growing degree days are a measure of yearly heat accumulation used to predict plant and animal development, and defined as the integral of warmth above a base temperature, discarding any excess above a maximum temperature. In this report, we use a base of 50°F and a cap of 86°F.
The average accumulated growing degree days in Palo Seco (El Gato) are rapidly increasing during April, increasing by 641°F, from 1,285°F to 1,926°F, over the course of the month.
Growing Degree Days in April
This section discusses the total daily incident shortwave solar energy reaching the surface of the ground over a wide area, taking full account of seasonal variations in the length of the day, the elevation of the Sun above the horizon, and absorption by clouds and other atmospheric constituents. Shortwave radiation includes visible light and ultraviolet radiation.
The average daily incident shortwave solar energy in Palo Seco (El Gato) is essentially constant during April, remaining within 0.2 kWh of 7.1 kWh throughout.
Average Daily Incident Shortwave Solar Energy in April
For the purposes of this report, the geographical coordinates of Palo Seco (El Gato) are 22.354 deg latitude, -100.192 deg longitude, and 3,652 ft elevation.
The topography within 2 miles of Palo Seco (El Gato) contains significant variations in elevation, with a maximum elevation change of 574 feet and an average elevation above sea level of 3,660 feet. Within 10 miles contains significant variations in elevation (2,346 feet). Within 50 miles contains large variations in elevation (7,008 feet).
The area within 2 miles of Palo Seco (El Gato) is covered by shrubs (91%), within 10 miles by shrubs (85%), and within 50 miles by shrubs (68%) and trees (23%).
This report illustrates the typical weather in Palo Seco (El Gato) year round, based on a statistical analysis of historical hourly weather reports and model reconstructions from January 1, 1980 to December 31, 2016.
Temperature and Dew Point
There is only a single weather station, Ponciano Arriaga International Airport, in our network suitable to be used as a proxy for the historical temperature and dew point records of Palo Seco (El Gato).
At a distance of 77 kilometers from Palo Seco (El Gato), closer than our threshold of 150 kilometers, this station is deemed sufficiently nearby to be relied upon as our primary source for temperature and dew point records.
The station records are corrected for the elevation difference between the station and Palo Seco (El Gato) according to the International Standard Atmosphere , and by the relative change present in the MERRA-2 satellite-era reanalysis between the two locations.
Please note that the station records themselves may additionally have been back-filled using other nearby stations or the MERRA-2 reanalysis.
All data relating to the Sun's position (e.g., sunrise and sunset) are computed using astronomical formulas from the book, Astronomical Tables of the Sun, Moon and Planets , by Jean Meeus.
All other weather data, including cloud cover, precipitation, wind speed and direction, and solar flux, come from NASA's MERRA-2 Modern-Era Retrospective Analysis . This reanalysis combines a variety of wide-area measurements in a state-of-the-art global meteorological model to reconstruct the hourly history of weather throughout the world on a 50-kilometer grid.
Land Use data comes from the Global Land Cover SHARE database , published by the Food and Agriculture Organization of the United Nations.
Elevation data comes from the Shuttle Radar Topography Mission (SRTM) , published by NASA's Jet Propulsion Laboratory.
Names, locations, and time zones of places and some airports come from the GeoNames Geographical Database .
Time zones for aiports and weather stations are provided by AskGeo.com .
Maps are © Esri, with data from National Geographic, Esri, DeLorme, NAVTEQ, UNEP-WCMC, USGS, NASA, ESA, METI, NRCAN, GEBCO, NOAA, and iPC.
The information on this site is provided as is, without any assurances as to its accuracy or suitability for any purpose. Weather data is prone to errors, outages, and other defects. We assume no responsibility for any decisions made on the basis of the content presented on this site.
We draw particular cautious attention to our reliance on the MERRA-2 model-based reconstructions for a number of important data series. While having the tremendous advantages of temporal and spatial completeness, these reconstructions: (1) are based on computer models that may have model-based errors, (2) are coarsely sampled on a 50 km grid and are therefore unable to reconstruct the local variations of many microclimates, and (3) have particular difficulty with the weather in some coastal areas, especially small islands.
We further caution that our travel scores are only as good as the data that underpin them, that weather conditions at any given location and time are unpredictable and variable, and that the definition of the scores reflects a particular set of preferences that may not agree with those of any particular reader.